Aerial Observations of Symmetric Instability at the NorthWall of the Gulf Stream
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An unusual spatial pattern on the ocean surface was captured by thermal airborne swaths taken across a strong sea surface temperature front at the NorthWall of the Gulf Stream. The thermal pattern on the cold side of the front resembles a staircase consisting of tens of steps, each up to ∼200 m wide and up to ∼0.3∘C warm. The steps are well organized, clearly separated by sharp temperature gradients, mostly parallel and aligned with the primary front. The interpretation of the airborne imagery is aided by oceanographic measurements from two research vessels. Analysis of the in situ observations indicates that the front was unstable to symmetric instability, a type of overturning instability that can generate coherent structures with similar dimensions to the temperature steps seen in the airborne imagery. It is concluded that the images capture, for the first time, the surface temperature field of symmetric instability turbulence.
The article of record as published may be found at http://dx.doi.org/10.1002/2017GL075735Data used in this paper are a subset of CASPER-East data set, hosted on https://researchworkspace.com/campaign/2560812/coupled-airsea-processes-and-em-ductingresearch-casper
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